Andrew Lockley and...@andrewlockley.com to me show details 12:22 AM
(10 hours ago)

>Do you have a reference for the two thirds?

Hi, Andrew -

Sure, I guess I should have put in a reference for the assertion.
Here's one example:


http://www.sciencemag.org/content/326/5953/716

Science 30 October 2009:
Vol. 326 no. 5953 pp. 716-718
DOI: 10.1126/science.1174760
REPORT
Improved Attribution of Climate Forcing to Emissions
Drew T. Shindell*, Greg Faluvegi, Dorothy M. Koch, Gavin A. Schmidt,
Nadine Unger and Susanne E. Bauer
+ Author Affiliations

NASA Goddard Institute for Space Studies and Columbia University, New
York, NY 10025, USA.
*To whom correspondence should be addressed. E-mail:
drew.t.shind...@nasa.gov


GISS material for the past several years has assumed this - I think
the first such paper goes back to @ 2006, actually,
but could be wrong on that.

I sometimes use a forcing pie chart in climate talks which I got from
Al Gore's Our Choice,
taken from a Shindell paper, which shows the percentage of +RF
respectively as:

CO2              43.1%
CH4              26.7%
BC                11.9%
Halocarbons    7.8%
CO & VOCs    6.7%
N2O               3.8%


I thought I read somewhere that it was assumed the IPCC AR5 would
reflect this,
but I don't know the current state of that.....perhaps Mike would know
that.....
but nothing would surprise me anymore....

All best,

Nathan





On Feb 24, 7:57 pm, Nathan Currier <natcurr...@gmail.com> wrote:
> Dear Robert,
>
> You wrote originally looking for help disputing a “skeptic,” and I
> hope it hasn’t been
> lost upon you that there sometimes seems to be almost as much
> disagreement within
> the climate community itself as between such “skeptics” and climate
> scientists. Indeed,
> the outcome of such internal disagreement could eventually be even
> more important for our fate
> than disputes with those who ultimately have little or no concern for
> science whatsoever.
>
> Perhaps the largest internal struggle in climate science regards
> methane. That is why David
> Archer recently wrote his strongly titled “Much Ado about Methane,”
> which Ken called one of
> the best recent pieces on methane emissions. I personally thought it
> was one of the most
> poorly conceived pieces of climate science from within the climate
> community, and the group AMEG –
> the Arctic Methane Emergency Group, formed from this Google
> geoengineering group – is still
> quite concerned with rebutting this piece of writing. I immediately
> started my own ongoing
> series in response, called Methane in the Twilight Zone, in which I
> address Archer’s “Much
> Ado” in some detail (particularly in Episode 2), and promptly received
> a private note of thanks
> from someone at the top of the climate heirarchy at NASA, specifically
> for those parts concerning
> Daivd Archer’s recent writing. So, you can see that there is,
> unfortunately, considerable
> disagreement on this!
>
> The reason, of course, is that methane feedbacks could potentially
> upend much of the worldview of
> many scientists, and could radically impact this topic of “non-
> linearity of climate sensitivity,” as well
> as the current state of the climate. You ask about Wasdell’s “ESS,”
> and about how it should
> impact considerations of geoengineering, but one of the greatest
> problems today is that this kind of “high-sensitivity”
> view, or any recognition that there could potentially be powerful
> tipping points at relatively short time scales,
> should impact both geoengineering policy AND emissions policy
> (particularly, in terms of advantaging and
> prioritizing immediate and large reductions of anthropogenic methane
> emissions).
>
> In terms of other things I noted within your various exchanges, the
> best recent work from NASA, now with a
> half-decade of pretty robust research behind it, suggests that the
> methane forcing is TWO THIRDS of CO2’s
> (added RF since industrialization, that is), not one third, as stated
> – thus, the recent human methane forcing
> is about twice as large as imagined at the time of the IPCC TAR, for
> example (exclusive of any earlier impacts
> on methane humans might have had).
>
> Further, in terms of whether there is evidence of increased methane
> releases in the arctic, I’ve printed below the
> NOAA data from Barrow, Alaska for a given day from the most recent
> year available, 2010. Methane spiked to
> 2230ppb that day there.  The question is really just what and where
> the precise source is, not that it is increasing
> and doing so quite rapidly.
>
> By the way, you said something at the beginning about reducing the CO2
> GWP –  but by definition, CO2’s GWP
> is always one, as perfect a numerical translation of monotheism as one
> could create, I guess.....
>
> Cheers, Nathan
>
> Methane at Barrow,  Alaska on 9/11/10
>
> BRW 2010 09 11 05  1909.11   6.13 .C.
> BRW 2010 09 11 06  1937.95  11.47 .C.
> BRW 2010 09 11 07  1952.57   5.80 .C.
> BRW 2010 09 11 08  1957.61   6.80 .C.
> BRW 2010 09 11 09  1935.10   4.13 .C.
> BRW 2010 09 11 10  1946.28   7.73 .C.
> BRW 2010 09 11 11  1976.60   7.42 .C.
> BRW 2010 09 11 12  1982.51   5.45 .C.
> BRW 2010 09 11 13  1989.94   3.03 .C.
> BRW 2010 09 11 14  1995.60   4.68 .C.
> BRW 2010 09 11 15  2009.41   3.65 .C.
> BRW 2010 09 11 16  2016.25   5.74 .C.
> BRW 2010 09 11 17  2039.49   8.05 .C.
> BRW 2010 09 11 18  2046.90  10.47 .C.
> BRW 2010 09 11 19  2039.67   3.53 .C.
> BRW 2010 09 11 20  2042.08   5.24 .C.
> BRW 2010 09 11 21  2058.38   7.64 .C.
> BRW 2010 09 11 22  2073.26   2.98 .C.
> BRW 2010 09 11 23  2074.07  21.03 .C.
> BRW 2010 09 12 00  2067.34  13.10 .C.
> BRW 2010 09 12 01  2005.53   1.39 .C.
> BRW 2010 09 12 02  1988.98  12.67 .C.
> BRW 2010 09 12 03  1965.76   4.13 .C.
> BRW 2010 09 12 04  1984.17  10.82 .C.
> BRW 2010 09 12 05  1956.75   4.72 .C.
> BRW 2010 09 12 06  1941.76   4.05 .C.
> BRW 2010 09 12 07  2051.73 112.21 .C.
> BRW 2010 09 12 08  2230.78  30.93 .C.
> BRW 2010 09 12 09  2181.13  35.70 .C.
> BRW 2010 09 12 10  2087.70  26.63 .C.
> BRW 2010 09 12 11  1968.64  30.33 .C.
> BRW 2010 09 12 12  1928.62   8.78 .C.
>
> For comparison, here is the same day on the first year of records
> there, 1987
> (note that it is not just lower, but also closer to the global average
> at the time):
>
> BRW 1987 09 11 05  -999.99 -99.99 *..
> BRW 1987 09 11 06  1797.62   7.26 .C.
> BRW 1987 09 11 07  -999.99 -99.99 *..
> BRW 1987 09 11 08  1814.18  18.15 .C.
> BRW 1987 09 11 09  -999.99 -99.99 *..
> BRW 1987 09 11 10  -999.99 -99.99 *..
> BRW 1987 09 11 11  1802.12   4.90 .C.
> BRW 1987 09 11 12  1803.20   8.48 .C.
> BRW 1987 09 11 13  1814.01  20.46 .C.
> BRW 1987 09 11 14  -999.99 -99.99 *..
> BRW 1987 09 11 15  1772.95   4.86 .C.
> BRW 1987 09 11 16  -999.99 -99.99 *..
> BRW 1987 09 11 17  1775.05   2.50 .C.
> BRW 1987 09 11 18  -999.99 -99.99 *..
> BRW 1987 09 11 19  1766.73   0.65 .C.
> BRW 1987 09 11 20  -999.99 -99.99 *..
> BRW 1987 09 11 21  -999.99 -99.99 *..
> BRW 1987 09 11 22  -999.99 -99.99 *..
> BRW 1987 09 11 23  -999.99 -99.99 *..
> BRW 1987 09 12 00  -999.99 -99.99 *..
> BRW 1987 09 12 01  -999.99 -99.99 *..
> BRW 1987 09 12 02  1768.09   1.55 ...
> BRW 1987 09 12 03  -999.99 -99.99 *..
> BRW 1987 09 12 04  -999.99 -99.99 *..
> BRW 1987 09 12 05  1782.46   1.00 ...
> BRW 1987 09 12 06  1776.73   1.12 ...
> BRW 1987 09 12 07  -999.99 -99.99 *..
> BRW 1987 09 12 08  1822.97  10.56 .C.
> BRW 1987 09 12 09  -999.99 -99.99 *..
> BRW 1987 09 12 10  1772.28  11.62 .C.
> BRW 1987 09 12 11  -999.99 -99.99 *..
> BRW 1987 09 12 12  1774.90   4.82 .C.
>
> On Feb 22, 4:23 pm, Robert Chris <r.g.ch...@open.ac.uk> wrote:
>
>
>
> > Ken
>
> > May I have your permission to quote your paragraph 'On the other hand
> > the Romans ...' in my PhD thesis.
>
> > This is about as good an exposition of the challenge of
> > intergenerational equity arsing from climate change that I could hope
> > to find and perfectly demonstrates the paradox of framing climate
> > change as an intergenerational problem.  We want to do right by them,
> > but who is them, the centennial them or the millennial them?  Why do
> > we assume that all future generations have the same interests, or if
> > we don't, on what basis do we favour one against another?  Why do we
> > tacitly assume that any future world with dramatically fewer people
> > would somehow not be as desirable as one with more or less the same
> > number as now?  The problem is that interesting as these and many
> > related questions are, they don't have easy answers that the whole
> > world will buy into as a basis for action.  So framing climate change
> > as an intergenerational problem introduces a slew of intellectual
> > challenges of the same order of complexity as the physical climate
> > science itself and create an Everest to climb before action can be
> > agreed.  How much easier if we forgot about the future and just agreed
> > amongst ourselves that the intrinsic indecency of fouling our nest and
> > squandering scarce resources is a sufficient reason for immediate
> > action.  Is that too much to ask?
>
> > That's a little polemical.  Hopefully it won't come out like that in
> > the thesis.
>
> > This thread has gone off in a direction I hadn't anticipated when it
> > started.  Many thanks to those who have contributed.  Don't let me
> > stop you if you want to continue.
>
> > Robert
>
> > On Feb 22, 4:38 pm, Ken Caldeira <kcalde...@carnegie.stanford.edu>
> > wrote:
>
> > > Both amounts and rates of change are important to estimating climate 
> > > damage.
>
> > > If we were turning the Earth into the Cretaceous over millions of years,
> > > that is not a problem.  If we are doing it in centuries, that is a 
> > > problem.
>
> > > So, if we are talking about near-term damage from climate change, the
> > > Charney sensitivity is the most relevant factor.
>
> > > If we are talking about long-term damage from a changed climate, then the
> > > Earth System sensitivity becomes relevant.
>
> > > I don't think God made the Earth with the perfect climate and that any
> > > cooling or warming is inherently bad. I do think the Earth is full of 
> > > stuff
> > > that is adapted to the current climate and that climate change is 
> > > damaging.
> > > So, I am more concerned with rates of change than absolute amounts of
> > > change.
>
> > > On the century scale of concern to most policy makers, rates and amounts 
> > > of
> > > change are closely linked.
>
> > > On the other hand, if the Romans had discovered fossil fuels and had a
> > > fossil-fueled industrial revolution, they would have maximized their net
> > > present value and we would be here two millennia later with rising seas,
> > > acidified oceans, melting ice caps, diminished biodiversity, etc, finding
> > > little solace in the fact that they followed the path their economists 
> > > told
> > > them was economically optimal. So, even the period with disruptive 
> > > climate *
> > > change* could last thousands of years and Earth System sensitivity becomes
> > > relevant on these time scales. However, once climate change stabilizes at 
> > > a
> > > new level, it is not clear to me that the changed climate itself is in any
> > > fundamental sense worse than what we started out with.
>
> > > From a policy perspective, this distinction between changing climate and a
> > > changed climate is of little interest, because the prescription is the 
> > > same
> > > in both cases:  *Stop using the atmosphere as a waste dump.
> > > *
>
> > > On Wed, Feb 22, 2012 at 3:30 AM, Robert Chris <r.g.ch...@open.ac.uk> 
> > > wrote:
> > > > Tom
>
> > > > Thanks for
>
> ...
>
> read more »

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